third hour exam id: eee105 password: prairie friday april 12 11 pm here 100 points (of 500 for...
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Third hour examThird hour exam
http://life.uiuc.edu/animalbiology/105/http://life.uiuc.edu/animalbiology/105/ID: eee105ID: eee105Password: prAIRiePassword: prAIRie
Friday April 12Friday April 1211 pm here11 pm here
100 points 100 points (of 500 for semester)(of 500 for semester)
29 questions29 questions 57 bubbles57 bubbles
If University-approved conflictIf University-approved conflictSign up with Karin NelsonSign up with Karin Nelson
by Wednesday’s lectureby Wednesday’s lecture
EEE 105
http://www.life.uiuc.edu/animalbiology/105/Name: eee105Password: prAIRie
SoilSoilSoilSoil
Ch. 14
SoilSoilSoilSoil
Ch. 14
Portion of the world not covered by water.
Land
Mixture of minerals, organic material, living organisms, air, and water
Soil
Soil FormationSoilSoilSoilSoil
Parent MaterialAncient rock layers with recent deposits from lava or glacial flows
Weathering
Fragmentation or chemical change of the parent material
Soil FormationSoilSoilSoilSoil
WeatheringMechanical
temperature changes & abrasion
Soil FormationSoilSoilSoilSoil
WeatheringMechanical
temperature changes & abrasion
Chemical
SoilSoilSoilSoilGlaciation
Wisconsin glaciation 18,000 years ago
SoilSoilSoilSoilGlaciation
soil deposition
SoilSoilSoilSoilGlaciation
soil deposition
moraines
SoilSoilSoilSoilGlaciation
soil deposition
moraines
Moraines formed of tillMoraines formed of till
SoilSoilSoilSoilGlaciation
soil deposition
morainesloess = wind blown dust
Soil FormationSoilSoilSoilSoil
WeatheringMechanical ChemicalBiologicalhumus = dead organic material
root hairs exchange nutrientsaerates , hydrates soil
Soil FormationSoilSoilSoilSoil
WeatheringMechanical ChemicalBiologicalhumus = dead organic material
root hairs exchange nutrientsaerates , hydrates soil
composting
Soil FormationSoilSoilSoilSoil
WeatheringMechanical ChemicalBiologicalhumus soil flora & fauna
earthworms
= dead organic material
Soil FormationSoilSoilSoilSoil
earthwormsCharles Darwin’s last book
The Formation of Vegetable Mould by the Action of Earthworms
Soil PropertiesSoil Properties• TextureTexture - Determined by the size of soil
particles.
– Too many large particles leads to extreme leaching.
– Too many small particles leads to poor drainage.
SoilSoilSoilSoil
SoilSoilSoilSoilSoil PropertiesSoil Properties
• TextureTexture
silt
clay
sand
Soil types characterized bySoil types characterized by% sand, silt, & clay% sand, silt, & clay
gravel 2 - 64 mm0.05 - 2mm
0.002 - 0.05 mm
< 0.002 mm
loess
• Soil Profile - A series of horizontal layers of different chemical composition, particle size, and amount of organic matter.
• Horizon - Each recognizable layer of the profile.
SoilSoilSoilSoil
• A Horizon - (Topsoil) Uppermost layer - contains most of the soil nutrients and organic matter.
• B Horizon - (Subsoil) Underneath topsoil. Contains less organic matter and fewer organisms, but accumulates nutrients leached from topsoil.
• C Horizon - Weathered parent material - very little organic material.
• A Horizon - (Topsoil) Uppermost layer - contains most of the soil nutrients and organic matter.
• B Horizon - (Subsoil) Underneath topsoil. Contains less organic matter and fewer organisms, but accumulates nutrients leached from topsoil.
• C Horizon - Weathered parent material - very little organic material.
SoilSoilSoilSoil
Grassland Soils
topsoil leaching
most root growth
A Horizon
low rainfall limits
A horizon supports
Usually a deep
Forest Soils
Topsoil thin
topsoil leachateforms a subsoil that supports
substantial root growth
• Mixtures ?– Over 15,000 separate soil types have
been classified in North America.
SoilSoilSoilSoil
Morrow PlotsMorrow Plots
SoilSoilSoilSoil
• Erosion - Wearing away and transportation of soil by wind and water.
SoilSoilSoilSoil
Worldwide removes 25.4 Billion tons/yr
Made worse by deforestation
Poor agricultural practices increase erosionand lead to the transport of associatedfertilizers and pesticides
and desertification
DesertificationDesertificationDesertificationDesertification
DesertificationDesertificationDesertificationDesertification
SoilSoilSoilSoil
Tombouctou, MaliTombouctou, Mali
19761976 19851985
DesertificationDesertificationDesertificationDesertification
DesertificationDesertificationDesertificationDesertification
• Climate change
• Deforestation
• Overgrazing
DesertificationDesertificationDesertificationDesertification
• The U.S.Inter-Mountain West
DesertificationDesertificationDesertificationDesertification
• The U.S.Inter-Mountain West
SalinizationSalinizationSalinizationSalinization
Calciu
mC
alcium
Sod
ium
Sod
ium
HH22OO
SalinizationSalinizationSalinizationSalinization
• Erosion - Wearing away and transportation of soil by wind and water.
SoilSoilSoilSoil
Worldwide removes 25.4 Billion tons/yr
Made worse by deforestation and desertification
Poor agricultural practices increase erosionand lead to the transport of associatedfertilizers and pesticides
• Erosion
SoilSoilSoilSoil
Most current agricultural areas lose topsoil faster than it can be replenished
Wind erosion
Water erosion
• Erosion - Wearing away and transportation of soil by wind and water.
SoilSoilSoilSoil
• Erosion
SoilSoilSoilSoil
• Erosion
SoilSoilSoilSoil
Sustainable farmingIllinois Erosion & Sediment Control Law
called “T by 2000”
T = tolerable soil loss
3-5 tons/acre/year
• Erosion
SoilSoilSoilSoil
Conservation tillage
Sustainable farming
• Erosion
SoilSoilSoilSoil
Conservation tillage
Sustainable farming
Hedgerows
• Erosion
SoilSoilSoilSoil
Conservation tillage
Sustainable farming
Hedgerows
Perimeter wetlands
• Erosion
SoilSoilSoilSoil
Great Plains have had four serious bouts of wind erosion since late 1800’s.